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JP3988828B2 - Dielectric constant measuring method and dielectric constant measuring apparatus - Google Patents
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JP3988828B2 - Dielectric constant measuring method and dielectric constant measuring apparatus - Google Patents

Dielectric constant measuring method and dielectric constant measuring apparatus Download PDF

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JP3988828B2
JP3988828B2 JP2004016855A JP2004016855A JP3988828B2 JP 3988828 B2 JP3988828 B2 JP 3988828B2 JP 2004016855 A JP2004016855 A JP 2004016855A JP 2004016855 A JP2004016855 A JP 2004016855A JP 3988828 B2 JP3988828 B2 JP 3988828B2
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dielectric constant
snow
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横山尚志
中田和一
斉 戸川
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AOMORI YAMADA GAKUEN EDUCATIONAL CORPORATION
Tokin Corp
Electronic Navigation Research Institute
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この発明は、アンテナから被測定物に向けて電波を照射し、その反射係数を測定して、被測定物の誘電率を算出する反射法による誘電率の測定方法及び誘電率測定装置に関し、特に積雪に人為的な作業を施すことなしに積雪の誘電率を測定することの出来る誘電率の測定方法及び誘電率測定装置に関するものである。   The present invention relates to a dielectric constant measuring method and a dielectric constant measuring apparatus by a reflection method in which a radio wave is irradiated from an antenna toward a measured object, a reflection coefficient thereof is measured, and a dielectric constant of the measured object is calculated. The present invention relates to a dielectric constant measuring method and a dielectric constant measuring apparatus that can measure the dielectric constant of snow without subjecting the snow to artificial work.

一般に、積雪は外部環境の変化により雪質と雪深が変化したり、又、その積雪の断面は層構造となり、その層構造内部の密度の変化等により誘電率が変化する。そして、現在、マイクロ波帯における積雪の誘電率を測定したデータはあるが、その他の周波数帯における測定データはなく、当然、誘電率を測定する測定装置も存在しない。そのため、発明者等は、平成11年青森空港において、一般的な誘電率測定法の1つである透過法により積雪の誘電率を測定した。   In general, the snow quality and snow depth of snow cover change due to changes in the external environment, and the cross section of the snow has a layer structure, and the dielectric constant changes due to changes in the density inside the layer structure. Currently, there is data that measured the dielectric constant of snow in the microwave band, but there is no measurement data in other frequency bands, and naturally there is no measuring device that measures the dielectric constant. Therefore, the inventors measured the dielectric constant of snow at 1999 Aomori Airport by the transmission method, which is one of the common dielectric constant measurement methods.

この透過法による積雪の誘電率測定装置は、図8に示すように、地面50に電波51が透過可能な透過ボード52が敷設され、この透過ボード52の下方(地下)には、電波51を透過ボード52面に向けて照射する送信用ホーンアンテナ53が設置されている。そして、透過ボード52の上方(地上)には、電波51(透過波)を受信する同様な形状の受信用ホーンアンテナ54が、支柱56に支持されて送信用ホーンアンテナ53に対向配置されている。そして、受信用ホーンアンテナ54には、透過波の透過特性を測定するネットワークアナライザ(図示せず)が接続されている。   As shown in FIG. 8, in this device for measuring the dielectric constant of snow by the transmission method, a transmission board 52 capable of transmitting radio waves 51 is laid on the ground 50, and the radio waves 51 are transmitted below the transmission board 52 (underground). A transmitting horn antenna 53 that irradiates the surface of the transmission board 52 is provided. Above the transmission board 52 (ground), a receiving horn antenna 54 having a similar shape for receiving the radio wave 51 (transmitted wave) is supported by the support 56 and disposed opposite the transmitting horn antenna 53. . The receiving horn antenna 54 is connected to a network analyzer (not shown) that measures the transmission characteristics of the transmitted wave.

このような構成で、透過ボード52上の積雪55に向けて電波51を照射すると、電波51は、積雪55と透過ボード52とを透過し、受信用ホーンアンテナ54で受信される。この受信された透過は、その透過特性がネットワークアナライザ(図示せず)により測定され、この透過特性から透過係数を算出し、積雪55の複素誘電率を求めている。
戸川斉他2名、」UHF帯での積雪の誘電率測定、2000年度日本雪氷学会全国大会予稿集、2000年9月20日、第165頁
In such a configuration, when the radio wave 51 is irradiated toward the snow cover 55 on the transmission board 52, the radio wave 51 passes through the snow cover 55 and the transmission board 52 and is received by the reception horn antenna 54. The transmission characteristics of the received transmission are measured by a network analyzer (not shown), a transmission coefficient is calculated from the transmission characteristics, and the complex dielectric constant of the snow cover 55 is obtained.
Akira Togawa and two others, "Measurement of dielectric constant of snow in UHF band, Proceedings of the 2000 Annual Meeting of the Japanese Society of Snow and Ice, September 20, 2000, p.165

このように構成されているので、気象や温度等の変動により、ネットワークアナライザ、同軸ケーブル(図示せず)等の測定機器はその電気的特性が変動し、測定誤差を生じる。従って、積雪55の誘電率を測定する前に、これらの測定機器を校正する必要がある。そのためには、まず、透過ボード52上に積もっている積雪55を除雪した後、透過ボード52のみの状態(積雪のない状態)で電波51を照射して、その透過波から測定機器を校正し、次いで、改めてもとのように積雪55を透過ボード52上に積み上げて平坦な積雪面を形成するという作業を行った後に、この積雪の透過特性を測定し、この透過特性から求めた透過係数から誘電率を算出する必要があった。   Since it is configured in this way, due to fluctuations in weather, temperature, etc., the measurement equipment such as a network analyzer and a coaxial cable (not shown) has its electric characteristics fluctuated, resulting in measurement errors. Therefore, before measuring the dielectric constant of the snow cover 55, it is necessary to calibrate these measuring instruments. For that purpose, first, after removing the snow 55 accumulated on the transmission board 52, the radio wave 51 is irradiated with only the transmission board 52 (no snow), and the measuring instrument is calibrated from the transmission waves. Then, after performing the work of stacking the snow cover 55 on the transmission board 52 to form a flat snow cover surface as before, the transmission characteristics of the snow cover are measured, and the transmission coefficient obtained from the transmission characteristics is measured. It was necessary to calculate the dielectric constant from

このように、測定しようとする積雪55に人為的な作業が施されるため、自然に降り積もった積雪55とは、積雪内部の密度が異なったものとなり、場所によって変化する。そのため、測定結果、周波数に対して誘電率の虚数部の誤差が大きく変化するという問題があった。   As described above, since the artificial work is performed on the snow cover 55 to be measured, the density inside the snow cover 55 is different from that of the snow cover 55 that has fallen naturally, and changes depending on the location. Therefore, the measurement result has a problem that the error of the imaginary part of the dielectric constant greatly changes with respect to the frequency.

さらに、測定に用いる電波51の周波数帯によっては、送信用及び受信用ホーンアンテナ53、54の形状が大きくなるため、それだけ風圧の影響が大きくなり、アンテナの振動や外来波により測定値が変動したり、又、受信用アンテナ54を支持する支柱56もそれだけ高くしなければならない等の問題があった。さらに、空港に設置してこのデータを積雪時における飛行コースのモニタ用に利用しようとすると、滑走路面からの高さ制限に抵触し設置出来ない等の問題があった。   Furthermore, depending on the frequency band of the radio wave 51 used for measurement, the shape of the transmitting and receiving horn antennas 53 and 54 becomes large, so that the influence of wind pressure increases, and the measured value fluctuates due to antenna vibration and external waves. In addition, there is a problem that the support column 56 that supports the receiving antenna 54 must be made higher. Furthermore, when it was installed at the airport and this data was used to monitor the flight course during snowfall, there was a problem that it could not be installed due to the height restriction from the runway surface.

請求項1に係る発明は、被測定物に電波を照射し、その反射波から被測定物の誘電率を算出する反射法による誘電率の測定方法において、電気的特性及び形状の等しい測定用送信アンテナと測定用受信アンテナとからなる測定用アンテナとこの測定用アンテナを同軸切換器に接続する同軸ケーブルとを有する測定系と、この測定系の電気的特性と等しい電気的特性を有し、同軸切換器に接続されたスルーの校正用伝送ケーブルとをそれぞれ備え、被測定物は積雪であり、
積雪を除去した初期校正時において、
(1)同軸切換器を測定用アンテナ側に切り換えて測定系における初期の校正特性をネットワークアナライザにより測定し、この初期の校正特性から測定系の初期の校正係数を求め、これを保存し、
(2)次いで、同軸切換器を校正用伝送ケーブル側に切り換えて、ネットワークアナライザにより校正特性を求め、この校正特性から校正系の初期の校正係数を求め、これを保存し、
(3)測定系の初期の校正係数から校正系の初期の校正係数を減算して、これを送受信アンテナ間透過係数値として保存し、
(4)測定用送信アンテナと測定用受信アンテナとの相対位置及び方向を一定にするとともに、反射板を除いた状態で、各(1)〜(3)の手順に従ってそれぞれアンテナ間結合係数を測定し、送信及び受信アンテナ間透過係数値からベクトル的に減算して、測定時校正値の初期値としてこれを保存し、
反射板上に積雪を載置した状態の測定時において、
)同軸切換器を校正用伝送ケーブル側に切り換えてネットワークアナライザにより校正特性を測定して、この校正特性から測定時における測定機器校正用の校正係数を求め、
)次いで、この測定機器校正用の校正係数と保存されている初期値との積を求め、これを測定時における測定機器校正用の真の反射係数としてネットワークアナライザに転送するとともに、測定データを追跡して、その反射係数を求め、
)この求めた反射係数から前記積雪の誘電率を算出し、
(8)この算出した積雪の誘電率から、VHF〜マイクロ波帯において導出されている実験式に基づいて、外挿法により測定に使用した電波の周波数帯から他の周波数帯における誘電率を算出するようにした誘電率の測定方法である。
According to a first aspect of the present invention, there is provided a method for measuring a dielectric constant by a reflection method in which a measured object is irradiated with a radio wave and a dielectric constant of the measured object is calculated from the reflected wave. A measuring system having a measuring antenna comprising an antenna and a receiving antenna for measurement, and a coaxial cable connecting the measuring antenna to a coaxial switch, and having an electrical characteristic equal to the electrical characteristic of the measuring system and being coaxial Each with a transmission cable for calibration of the through connected to the switch, the object to be measured is snow,
During initial calibration after removing snow ,
(1) Switch the coaxial switch to the measurement antenna side, measure the initial calibration characteristics in the measurement system with a network analyzer, obtain the initial calibration coefficient of the measurement system from the initial calibration characteristics, save this,
(2) Next, the coaxial switch is switched to the calibration transmission cable side, the calibration characteristic is obtained by a network analyzer, the initial calibration coefficient of the calibration system is obtained from this calibration characteristic, and this is stored.
(3) The initial calibration coefficient of the calibration system is subtracted from the initial calibration coefficient of the measurement system, and this is stored as a transmission coefficient value between the transmitting and receiving antennas.
(4) The relative position and direction of the measurement transmitting antenna and the measurement receiving antenna are made constant, and the coupling coefficient between antennas is measured according to the procedures of (1) to (3) with the reflector removed. Subtract the vector from the transmission coefficient between the transmission and reception antennas, save this as the initial value of the calibration value at the time of measurement,
At the time of measuring the state where snow is placed on the reflector,
( 5 ) Switch the coaxial switch to the calibration transmission cable side, measure the calibration characteristics with a network analyzer, and obtain the calibration coefficient for measuring equipment calibration at the time of measurement from this calibration characteristics.
( 6 ) Next, the product of the calibration coefficient for calibration of the measuring instrument and the stored initial value is obtained, and this is transferred to the network analyzer as a true reflection coefficient for calibration of the measuring instrument at the time of measurement. To find its reflection coefficient,
( 7 ) The dielectric constant of the snow is calculated from the obtained reflection coefficient ,
(8) From the calculated dielectric constant of snow, based on the empirical formula derived in the VHF to microwave band, the dielectric constant in other frequency bands is calculated from the frequency band of the radio wave used for measurement by extrapolation. This is a method for measuring the dielectric constant.

請求項に係る発明は、被測定物に電波を照射し、その反射波から被測定物の誘電率を算出する反射法による誘電率測定装置において、被測定物は電波を反射する反射板上に降り積もった積雪であり、電気的特性及び形状の等しい測定用送信アンテナと測定用受信アンテナとからなる測定用アンテナと、この測定用アンテナを同軸切換器に接続する同軸ケーブルと測定用アンテナとを有する測定系が構成され、この測定系の電気的特性と等しい電気的特性を有し、同軸切換器に接続されたスルーの校正用伝送ケーブルと、ネットワークアナライザに接続され、校正用伝送ケーブルと測定系とを切り換える手段を有する同軸切換器と、この同軸切換器を介して校正用伝送ケーブルと測定系とに接続されているとともに、校正用伝送ケーブル及び測定系からの校正特性と測定系からの反射特性及びアンテナ間結合特性を測定するネットワークアナライザと、反射特性、校正特性からそれぞれ校正係数、反射係数を算出する機能と、測定機器校正値の初期値を求める機能と、これらの値を保存する機能と、測定した積雪の反射係数からこの積雪の誘電率を算出する機能と、算出した積雪の誘電率から、VHF〜マイクロ波帯において導出されている実験式に基づいて、外挿法により測定に使用した電波の周波数帯から他の周波数帯に換算する機能とを備えたパソコンを有する誘電率測定装置である。 The invention according to claim 2 irradiates radio waves to the measurement object, the dielectric constant measuring apparatus according to the reflection method of calculating the dielectric constant of the object to be measured from the reflected wave, the object to be measured is reflecting board for reflecting radio waves A measurement antenna comprising a measurement transmission antenna and a measurement reception antenna having the same electrical characteristics and shape, a coaxial cable connecting the measurement antenna to a coaxial switch, and a measurement antenna. A measurement system is configured and has electrical characteristics equal to the electrical characteristics of the measurement system. The through calibration transmission cable connected to the coaxial switch, and the network analyzer connected to the calibration transmission cable and measurement. A coaxial switch having means for switching between the system, the calibration transmission cable and the measurement system via the coaxial switch, and a calibration transmission cable and Network analyzer that measures the calibration characteristics from the stationary system, the reflection characteristics from the measurement system, and the coupling characteristics between the antennas, the function to calculate the calibration coefficient and the reflection coefficient from the reflection characteristics and the calibration characteristics, respectively, and the initial value of the measurement equipment calibration value a function of obtaining and a function of storing these values, the function of calculating the dielectric constant of the snow from the reflection coefficients of the measured snow, dielectric constant of the calculated snow, are derived in VHF~ microwave band A dielectric constant measuring apparatus having a personal computer having a function of converting a frequency band of radio waves used for measurement by an extrapolation method into another frequency band based on an empirical formula .

請求項に係る発明は、請求項2に記載の誘電率測定装置において、電波の周波数は、Cバンドを用いた誘電率測定装置である。 The invention according to claim 3 is the dielectric constant measuring apparatus according to claim 2, wherein the frequency band of the radio wave uses a C band.

請求項1及び請求項2に係わる発明は、測定機器の校正時に、反射板上の積雪を除去する必要がなく、手間がかからない。特に、積雪の誘電率を測定する場合には、従来のように、積雪に人為的な作業を施す必要がないので、積雪内部の密度も自然の状態のものが得られ、外気温や日商の変化等により変動する自然の積雪に対する誘電率を正確に測定出来る。 In the inventions according to claims 1 and 2, it is not necessary to remove the snow cover on the reflecting plate at the time of calibration of the measuring device, and it does not take time. In particular, when measuring the dielectric constant of snow, it is not necessary to perform artificial work on the snow as in the past, so the density inside the snow can be obtained in a natural state, and the outside temperature and daily It is possible to accurately measure the dielectric constant for natural snow that fluctuates due to changes in snow.

その上、測定用アンテナや同軸ケーブル等の測定データに影響を与える測定機器を屋外に設置し、長期間の測定の場合にも、周囲の環境温度変化による同軸ケーブルの伸縮を考慮する必要がなく、従って、校正系と測定系との電気的特性が相違することもなくなる。又、測定用送信及び受信アンテナ間の直接受信波による影響も除去することが出来る。さらに、実施例1における校正系の反射板の周囲に形成される雪の壁面による反射波が受信されてしまうことにより生じる問題もなくなり、それだけ測定精度も良くなる。その上、装置自体が簡略なものとなり、又、校正時においても積雪には全く手作業を加える必要がない等の効果がある。 In addition, measurement devices such as antennas for measurement and coaxial cables are installed outdoors, and there is no need to consider the expansion and contraction of coaxial cables due to changes in the ambient temperature even when measuring for long periods. Therefore, the electrical characteristics of the calibration system and the measurement system do not differ. In addition, the influence of the direct reception wave between the transmission for measurement and the reception antenna can be eliminated. Furthermore, there is no problem caused by reception of a reflected wave from the wall surface of the snow formed around the calibration system reflector in the first embodiment, and the measurement accuracy is improved accordingly. In addition, the apparatus itself is simplified, and there is an effect that it is not necessary to add any manual work to the snow cover even during calibration.

さらに、請求項1及び請求項2に係る発明は、反射効率が良くなり、又、乱反射による反射波の拡散も少なくなる。その上、反射板上に自然に降り積もった積雪の誘電率を、常にリアルタイムで正確に測定することが出来る。 Further, the inventions according to claims 1 and 2 improve the reflection efficiency and also reduce the diffusion of reflected waves due to irregular reflection. In addition, the dielectric constant of the snow that naturally falls on the reflector can always be measured accurately in real time.

請求項3に係わる発明は、請求項1及び請求項2に係る発明と同様な効果がある。さらに、測定用アンテナの形状を小型化出来る周波数帯(例えば、Cバンド)を用いて測定し、これを求める周波数帯(例えば、ILSのグライドパス周波数)に換算することが出来るので、形状の大きなアンテナ等を用いる必要がない。従って、従来のように、風圧の影響によるアンテナの振動や外来波により測定値の変動、又、測定用アンテナの高さ等の問題を除去することが出来る。その上、測定機器の校正時における反射板上の積雪を除去する必要は全くなく、常にリアルタイムで誘電率をより正確に測定することが出来る。 The invention according to claim 3 has the same effect as the inventions according to claim 1 and claim 2. Furthermore, since the measurement antenna can be measured using a frequency band that can reduce the size (for example, C band) and can be converted into a desired frequency band (for example, ILS glide path frequency), the shape of the antenna is large. There is no need to use an antenna or the like. Therefore, as in the prior art, it is possible to eliminate problems such as variations in measured values due to antenna vibration and external waves due to the influence of wind pressure, and the height of the measurement antenna. In addition, there is no need to remove snow on the reflector during calibration of the measuring instrument, and the dielectric constant can always be measured more accurately in real time.

被測定物に電波を照射し、その反射波から被測定物の誘電率を算出する反射法による誘電率の測定方法において、電気的特性及び形状の等しい測定用送信アンテナと測定用受信アンテナとからなる測定用アンテナとこの測定用アンテナを同軸切換器に接続する同軸ケーブルとを有する測定系と、この測定系の電気的特性と等しい電気的特性を有し、同軸切換器に接続されたスルーの校正用伝送ケーブルとをそれぞれ備え、被測定物は積雪であり、積雪を除去した初期校正時において、
(1)同軸切換器を測定用アンテナ側に切り換えて測定系における初期の校正特性をネットワークアナライザにより測定し、この初期の校正特性から測定系の初期の校正係数を求め、これを保存し、
(2)次いで、同軸切換器を校正用伝送ケーブル側に切り換えて、ネットワークアナライザにより校正特性を求め、この校正特性から校正系の初期の校正係数を求め、これを保存し、
(3)測定系の初期の校正係数から校正系の初期の校正係数を減算して、これを送受信アンテナ間透過係数値として保存し、
(4)測定用送信アンテナと測定用受信アンテナとの相対位置及び方向を一定にするとともに、反射板を除いた状態で、各(1)〜(3)の手順に従ってそれぞれアンテナ間結合係数を測定し、送信及び受信アンテナ間透過係数値からベクトル的に減算して、測定時校正値の初期値としてこれを保存し、
反射板上に積雪を載置した状態の測定時において、
)同軸切換器を校正用伝送ケーブル側に切り換えてネットワークアナライザにより校正特性を測定して、この校正特性から測定時における測定機器校正用の校正係数を求め、
)次いで、この測定機器校正用の校正係数と保存されている初期値との積を求め、これを測定時における測定機器校正用の真の反射係数としてネットワークアナライザに転送するとともに、測定データを追跡して、その反射係数を求め、
)この求めた反射係数から前記積雪の誘電率を算出し、
(8)この算出した積雪の誘電率から、VHF〜マイクロ波帯において導出されている実験式に基づいて、外挿法により測定に使用した電波の周波数帯から他の周波数帯における誘電率を算出するようにした。
In a method for measuring a dielectric constant by a reflection method in which a measured object is irradiated with radio waves and the dielectric constant of the measured object is calculated from the reflected wave, a measurement transmitting antenna and a measuring receiving antenna having the same electrical characteristics and shape are used. A measurement system having a measurement antenna and a coaxial cable connecting the measurement antenna to the coaxial switch, and an electrical characteristic equal to the electrical characteristic of the measurement system, Each with a calibration transmission cable, and the object to be measured is snow, and during initial calibration after removing snow ,
(1) Switch the coaxial switch to the measurement antenna side, measure the initial calibration characteristics in the measurement system with a network analyzer, obtain the initial calibration coefficient of the measurement system from the initial calibration characteristics, save this,
(2) Next, the coaxial switch is switched to the calibration transmission cable side, the calibration characteristic is obtained by a network analyzer, the initial calibration coefficient of the calibration system is obtained from this calibration characteristic, and this is stored.
(3) The initial calibration coefficient of the calibration system is subtracted from the initial calibration coefficient of the measurement system, and this is stored as a transmission coefficient value between the transmitting and receiving antennas.
(4) The relative position and direction of the measurement transmitting antenna and the measurement receiving antenna are made constant, and the coupling coefficient between antennas is measured according to the procedures of (1) to (3) with the reflector removed. Subtract the vector from the transmission coefficient between the transmission and reception antennas, save this as the initial value of the calibration value at the time of measurement,
At the time of measuring the state where snow is placed on the reflector,
( 5 ) Switch the coaxial switch to the calibration transmission cable side, measure the calibration characteristics with a network analyzer, and obtain the calibration coefficient for measuring equipment calibration at the time of measurement from this calibration characteristics.
( 6 ) Next, the product of the calibration coefficient for calibration of the measuring instrument and the stored initial value is obtained, and this is transferred to the network analyzer as a true reflection coefficient for calibration of the measuring instrument at the time of measurement. To find its reflection coefficient,
( 7 ) The dielectric constant of the snow is calculated from the obtained reflection coefficient ,
(8) From the calculated dielectric constant of snow, based on the empirical formula derived in the VHF to microwave band, the dielectric constant in other frequency bands is calculated from the frequency band of the radio wave used for measurement by extrapolation. I tried to do it.

この発明の第1の実施例は、ネットワークアナライザや同軸ケーブルなどの測定機器を校正するための一対の校正用アンテナを含む校正系と一対の測定用アンテナを含む測定系との2系統を構成するとともに、この2系統はいずれも電気的特性が同一となるように、アンテナ、同軸ケーブルのケーブル長、損失及びアンテナ高、形状等すべて等しくなるように構成し、ネットワークアナライザで被測定物の反射特性を測定して、この反射特性から反射係数を算出し被測定物の誘電率εを算出するようにした実施例を示すもので、以下、図1に基づいて説明する。   The first embodiment of the present invention constitutes two systems, a calibration system including a pair of calibration antennas for calibrating a measuring instrument such as a network analyzer and a coaxial cable, and a measurement system including a pair of measurement antennas. In addition, these two systems are configured so that the antenna, coaxial cable cable length, loss and antenna height, shape, etc. are all equal so that the electrical characteristics of both systems are the same, and the reflection characteristics of the object to be measured by the network analyzer 1 is measured, and the reflection coefficient is calculated from the reflection characteristics to calculate the dielectric constant ε of the object to be measured, which will be described below with reference to FIG.

図1は、この発明の第1の実施例を示すもので、1(1a、1b)は、電気的特性及び形状が同一の対をなす測定用アンテナで、信号源(図示せず)からの電波2を、地面6に設置されている金属製の反射板7上に載置されている被測定物3へ照射する測定用送信アンテナ1aと被測定物3からの反射波4を受信する測定用受信アンテナ1bとにより構成されており、この実施例の場合にはホーンアンテナが用いられている。   FIG. 1 shows a first embodiment of the present invention. Reference numerals 1 (1a, 1b) denote measurement antennas having the same electrical characteristics and shape, and from a signal source (not shown). Measurement transmitting antenna 1a for irradiating the object 3 to be measured 3 placed on the metal reflector 7 installed on the ground 6 and measurement for receiving the reflected wave 4 from the object 3 For this embodiment, a horn antenna is used.

5(5a、5b)は電気的特性及び形状が同一の対をなす校正用アンテナで、測定用アンテナ1とも電気的特性及び形状が同一である。この校正用アンテナ5(5a、5b)は、地面6に設置されている金属製の反射板8に向けて電波2を照射する校正用送信アンテナ5aと反射板8からの反射波を受信する校正用受信アンテナ5bとにより構成されている。   5 (5a, 5b) is a calibration antenna having a pair having the same electrical characteristics and shape, and the measurement antenna 1 has the same electrical characteristics and shape. The calibration antenna 5 (5a, 5b) is a calibration transmitting antenna 5a that irradiates a radio wave 2 toward a metal reflector 8 installed on the ground 6 and a calibration that receives a reflected wave from the reflector 8. And the receiving antenna 5b.

なお、この実施例では、電波2の測定周波数帯域はCバンドで、測定用及び校正用アンテナとしてはホーンアンテナを用い、誘電率を測定するための被測定物3としては、反射板7上に降り積もった積雪(以下、積雪3とも記す)とした。この実施例では、被測定物3としては、積雪3で測定したが、これに限定されることなく、その他の誘電物質も同様に測定することが出来る。   In this embodiment, the measurement frequency band of the radio wave 2 is a C band, a horn antenna is used as a measurement and calibration antenna, and a device under test 3 for measuring a dielectric constant is provided on a reflector 7. It was assumed that the snowfall was piled up (hereinafter also referred to as snowfall 3). In this embodiment, the object to be measured 3 is measured by the snow cover 3, but is not limited to this, and other dielectric materials can be measured in the same manner.

反射板7、8は、電波を反射する金属製であり、反射効率を上げるためのもので、校正系側及び測定系側とも地面6に設置されている。なお、この実施例の場合には、校正系に設置されている反射板8には、加熱装置(図示せず)が接続されており、雪の降る季節には、常時加熱して反射板8の表面に雪が積もらないように構成されている。測定系の反射板7には、被測定物3である自然な積雪が形成される。   The reflection plates 7 and 8 are made of metal that reflects radio waves and are for increasing the reflection efficiency, and are installed on the ground 6 on both the calibration system side and the measurement system side. In the case of this embodiment, a heating device (not shown) is connected to the reflection plate 8 installed in the calibration system, and the reflection plate 8 is always heated during the snowy season. It is configured so that snow does not accumulate on the surface. On the reflection plate 7 of the measurement system, natural snow as the object to be measured 3 is formed.

測定用アンテナ1と校正用アンテナ5とは、いずれも2本の支柱9、10に掛け渡されたポール11の中心線から等距離の位置に水平方向に可動可能に取り付けられている。その際、測定用アンテナ1は、被測定物3の上方に取り付けられているとともに、測定用送信アンテナ1aと測定用受信アンテナ1bとの設置角度は、測定用送信アンテナ1aから放射された電波がすべて被測定物3で反射して測定用受信アンテナ1bで受信され、直接波4aが受信されないように設置されている。なお、破線で示す電波は、被測定物3を透過して反射板7で反射される透過波を示している。   Both the measurement antenna 1 and the calibration antenna 5 are mounted so as to be movable in the horizontal direction at positions equidistant from the center line of the pole 11 spanned between the two supports 9 and 10. At that time, the measurement antenna 1 is attached above the DUT 3 and the installation angle between the measurement transmission antenna 1a and the measurement reception antenna 1b is such that the radio wave radiated from the measurement transmission antenna 1a is All are reflected by the device under test 3 and received by the measurement receiving antenna 1b so that the direct wave 4a is not received. A radio wave indicated by a broken line indicates a transmitted wave that passes through the DUT 3 and is reflected by the reflecting plate 7.

同様に、校正用アンテナ5は、反射板8の上方に取り付けられており、校正用送信アンテナ5aと校正用受信アンテナ5bとの設置角度は、上記測定用アンテナ1と同様に校正用送信アンテナ5aから放射された電波2がすべて反射板8で反射して校正用受信アンテナ5bで受信され、直接波4aが受信されないように設置されている。   Similarly, the calibration antenna 5 is mounted above the reflector 8, and the installation angle between the calibration transmission antenna 5 a and the calibration reception antenna 5 b is the same as that of the measurement antenna 1. The radio wave 2 radiated from is reflected by the reflecting plate 8 and received by the calibration receiving antenna 5b, so that the direct wave 4a is not received.

なお、この実施例の場合には、支柱9、10は、2本使用しているが、これを1本の支柱とし、これにポール11の中心部を固定し、このポール11の両端部にそれぞれ測定用アンテナ1と校正用アンテナ5とを取り付けて支柱を中心としてその両側に測定系と校正系とを配置するように構成してもよい。   In this embodiment, two support columns 9 and 10 are used. However, this is used as one support column, and the center portion of the pole 11 is fixed to the support column. The measurement antenna 1 and the calibration antenna 5 may be attached to each other, and the measurement system and the calibration system may be arranged on both sides around the support column.

12は同軸切換器で、ネットワークアナライザ15に接続されているとともに、測定系と校正系とを切り換える手段を有し、測定系同軸ケーブル13及び校正系同軸ケーブル14を介して測定用及び校正用アンテナ1、5に接続されている。なお、測定系は、測定系同軸ケーブル13、測定用アンテナ1等により構成されており、校正系は、校正系同軸ケーブル14、校正用アンテナ5等により構成されている。   A coaxial switch 12 is connected to the network analyzer 15 and has means for switching between the measurement system and the calibration system. The measurement and calibration antennas are connected via the measurement system coaxial cable 13 and the calibration system coaxial cable 14. 1 and 5 are connected. The measurement system includes a measurement system coaxial cable 13 and a measurement antenna 1 and the calibration system includes a calibration system coaxial cable 14 and a calibration antenna 5 and the like.

ネットワークアナライザ15は、反射波の反射特性を測定するもので、同軸切換器12により測定系と校正系とを切り換え、それぞれ測定用受信アンテナ1b及び校正用受信アンテナ5bで受信された被測定物3及び反射板8からの反射波の反射特性がそれぞれ測定されている。16はパソコンで、ネットワークアナライザ15で測定された測定系及び校正系における反射特性の測定結果から、それぞれ反射係数が算出され、次いで、この求めた反射係数から被測定物3の誘電率εが算出される。   The network analyzer 15 measures the reflection characteristics of the reflected wave. The coaxial switch 12 switches between the measurement system and the calibration system, and the device under test 3 received by the measurement receiving antenna 1b and the calibration receiving antenna 5b, respectively. The reflection characteristics of the reflected wave from the reflector 8 are measured. Reference numeral 16 denotes a personal computer, and the reflection coefficient is calculated from the measurement results of the reflection characteristics in the measurement system and the calibration system measured by the network analyzer 15, and then the dielectric constant ε of the DUT 3 is calculated from the obtained reflection coefficient. Is done.

次に、実際に被測定物3として反射板7上に自然に降り積もった積雪(以下、積雪3と記す)の誘電率εを求める場合について説明する。
ここで、測定系の反射板7上には、自然に雪が降り積もり積雪3が形成されており、校正系の反射板8は常時加熱されており、従って、反射板8上には積雪3はない状態であるとする。そこで、測定系の反射板7上に積もった積雪3の誘電率εを求めるためには、上記の装置を用いて積雪3の反射特性を測定し、この反射特性から反射係数を求め、この反射係数から誘電率を算出しなければならない。
Next, a description will be given of a case where the dielectric constant ε of the snow that has actually fallen naturally on the reflector 7 as the object to be measured 3 (hereinafter referred to as snow 3) is obtained.
Here, snow falls naturally on the reflection plate 7 of the measurement system, and the snow cover 3 is formed, and the reflection plate 8 of the calibration system is always heated. Therefore, there is no snow cover 3 on the reflection plate 8. Suppose that it is in a state. Therefore, in order to obtain the dielectric constant ε of the snow cover 3 accumulated on the reflection plate 7 of the measurement system, the reflection characteristics of the snow cover 3 are measured using the above-described device, the reflection coefficient is obtained from the reflection characteristics, and this reflection The dielectric constant must be calculated from the coefficient.

先ず、気象条件や温度変化等によりネットワークアナライザ15や測定系同軸ケーブル13、校正系同軸ケーブル14の伸縮等により測定機器の電気的特性が変動するため、これら測定機器の校正が行われる。この場合、校正系における反射板8上には、積雪がない状態で行われる。この実施例の場合には、校正系の反射板8は常時加熱されているので、表面に積雪はない。そこで、同軸切換器12を校正系に切り換えて電波2を校正用送信アンテナ5aから照射すると、反射板8からの反射波は、校正用受信アンテナ5bで受信され、ネットワークアナライザ15でその反射特性が測定される。校正時において測定された反射特性から反射係数が求められ、これによりネットワークアナライザ15や測定系同軸ケーブル13及び校正系同軸ケーブル14等の測定機器が校正される。   First, since the electrical characteristics of the measuring device fluctuate due to expansion and contraction of the network analyzer 15, the measurement system coaxial cable 13, and the calibration system coaxial cable 14 due to weather conditions and temperature changes, the measurement devices are calibrated. In this case, it is performed in a state where there is no snow on the reflection plate 8 in the calibration system. In the case of this embodiment, since the calibration reflector 8 is always heated, there is no snow on the surface. Therefore, when the coaxial switch 12 is switched to the calibration system and the radio wave 2 is irradiated from the calibration transmitting antenna 5a, the reflected wave from the reflecting plate 8 is received by the calibration receiving antenna 5b and the reflection characteristic of the reflected wave is received by the network analyzer 15. Measured. A reflection coefficient is obtained from the reflection characteristics measured at the time of calibration, and thereby the measurement equipment such as the network analyzer 15, the measurement system coaxial cable 13, and the calibration system coaxial cable 14 is calibrated.

次いで、同軸切換器12を測定系に切り換え、測定用送信アンテナ1aから電波2を反射板7上の積雪3面に照射して、その反射波を同様にして測定用受信アンテナ1bで受信し、ネットワークアナライザ15により反射特性が測定される。このように、測定された反射特性から、同様に積雪時における反射係数が求められる。この反射係数から積雪3の誘電率が算出される。このように、測定時には反射特性を測定し、この反射特性から反射係数が求められる。校正時には同軸切換器12により校正用アンテナ5に切り換えて時間経過・外気温の変化による測定系のドリフトをその都度校正し、次いで、同軸切換器12を測定系に切り換えて、測定時における反射特性を測定し、この反射特性から反射係数が求められ、長期的に積雪3の誘電率の変化を測定することが出来る。   Next, the coaxial switch 12 is switched to the measurement system, the radio wave 2 is irradiated from the measurement transmission antenna 1a onto the snow cover 3 on the reflection plate 7, and the reflected wave is similarly received by the measurement reception antenna 1b. The reflection characteristic is measured by the network analyzer 15. In this way, the reflection coefficient during snow accumulation is similarly obtained from the measured reflection characteristics. The dielectric constant of the snow cover 3 is calculated from this reflection coefficient. As described above, the reflection characteristic is measured at the time of measurement, and the reflection coefficient is obtained from the reflection characteristic. At the time of calibration, the coaxial switch 12 is switched to the calibration antenna 5 to calibrate the measurement system drift due to the passage of time and the change of the outside air temperature each time. The reflection coefficient is obtained from this reflection characteristic, and the change in the dielectric constant of the snow cover 3 can be measured over the long term.

上記のようにして算出された積雪3の誘電率は、Cバンドの周波数帯で測定された結果であるので、VHF〜マイクロ波帯における特定周波数で測定され実験的に導出されている下記実験式に基づいて、外挿法により空港に設置されているグライドパスの周波数帯に換算した誘電率が算出する。以下、特定周波数(VHF〜マイクロ波帯)で測定された積雪複素誘電率を任意周波数における誘電率に換算する換算法について説明する。   Since the dielectric constant of the snow cover 3 calculated as described above is a result of measurement in the C band frequency band, the following empirical formula is measured and experimentally derived at a specific frequency in the VHF to microwave band. Based on the above, the dielectric constant converted to the frequency band of the glide path installed at the airport is calculated by extrapolation. Hereinafter, a conversion method for converting the snow complex permittivity measured at a specific frequency (VHF to microwave band) into a permittivity at an arbitrary frequency will be described.

水分を含む積雪の分散特性がDebyの式で与えられる水の分散特性に対応して表現出来ると仮定して、周波数fにおける積雪誘電率虚数部ε"s(f)及び積雪誘電率実数部ε's(f)の増分Δε's(f)は、それぞれ下記の(A)式及び(B)式を用いる。   Assuming that the dispersion characteristics of snow containing moisture can be expressed in correspondence with the dispersion characteristics of water given by the Deby equation, the imaginary part ε "s (f) of the snow cover dielectric constant at the frequency f and the real part ε's of the snow cover dielectric constant For the increment Δε ′s (f) of (f), the following equations (A) and (B) are used, respectively.

Figure 0003988828
Figure 0003988828

Figure 0003988828
Figure 0003988828

ここで、ε"sは積雪誘電率虚数部、Δε'sは積雪水分による積雪誘電率実数部ε'sの増分で、ε's=ε'd+Δε'sである。(但し、ε'dは水の占有体積を空気で置き換え乾雪とした時の誘電率実数部)である。又、fは純水の誘電緩和周波数で、f=8.84(GHz)であり、tan
δwは純水の誘電正接(損失係数)で、温度0℃では、下記(C)式となる。
Here, ε "s is the imaginary part of the snow permittivity, Δε's is the increment of the snow permittivity real part ε's due to the snow moisture, and ε's = ε'd + Δε's (where ε'd is the volume occupied by water) The real part of the dielectric constant when air is replaced with dry snow.) F 0 is the dielectric relaxation frequency of pure water, f 0 = 8.84 (GHz), and tan
δw is a dielectric loss tangent (loss factor) of pure water, and at a temperature of 0 ° C., the following equation (C) is obtained.

Figure 0003988828
Figure 0003988828

ここで、周波数fにおける複素誘電率の実数部及び虚数部の測定値を、それぞれε's(f)、ε"s(f)とすれば、任意の周波数fにおける積雪3の複素誘電率の虚数部は、(A)式を用いると、下記(D)式で表される。 Here, the measurement value of the real part and the imaginary part of the complex dielectric constant at a frequency f M, respectively ε's (f M), ε " if s (f M), the complex dielectric constant of the snow 3 at an arbitrary frequency f The imaginary part of is represented by the following equation (D) using equation (A).

Figure 0003988828
Figure 0003988828

次いで、積雪3の複素誘電率の実数部は、上記ε's=ε'd+Δε'sから(A)、(B)、(C)式を用いて、下記(E)式で表される。   Next, the real part of the complex permittivity of the snow cover 3 is expressed by the following equation (E) using the equations (A), (B), and (C) from the above ε's = ε'd + Δε's.

Figure 0003988828
Figure 0003988828

ここで、発明者等は、3〜37(GHz)のマイクロ波帯の周波数で報告されているHallikainmenn等の実験式が、3(GHz)以下の周波数帯に対しても有効であると仮定し、0〜5(GHz)の帯域で、体積含水率0〜12(%)、密度0.25(g/cm3)の積雪の誘電率を計算した結果を、図2、図3に実線で示した。このデータで、f=5(GHz)における複素誘電率を既知の測定値と仮定し、(D)、(E)式から新たにf<5(GHz)の周波数について複素誘電率を算出した結果をマーカプロットした。この結果から明らかであるように、両者は良く一致していることが判明した。   Here, the inventors assume that the empirical formula of Hallikainmenn et al. Reported in the frequency band of 3 to 37 (GHz) is also effective for the frequency band of 3 (GHz) or lower. The results of calculating the dielectric constant of the snow cover having a volume water content of 0 to 12 (%) and a density of 0.25 (g / cm 3) in the 0 to 5 (GHz) band are shown by solid lines in FIGS. With this data, assuming that the complex permittivity at f = 5 (GHz) is a known measured value, the result of newly calculating the complex permittivity for the frequency f <5 (GHz) from the equations (D) and (E) A marker plot was made. As is clear from this result, it was found that both agree well.

このようにして積雪3の誘電率を求めたので、従来のようにネットワークアナライザ15の校正をする際に、反射板8上の積雪を除雪して測定機器の校正時における反射特性を測定し、この反射特性から反射係数を求めて校正値を求めた後に、再度、測定時に平坦な積雪面にする作業が必要であったが、この作業が必要なくなる。そのため、人為的な作業による積雪内部の密度の変動をなくすことが出来、より正確な自然積雪による測定データを得ることが出来る。   Thus, since the dielectric constant of the snow cover 3 was obtained, when the network analyzer 15 was calibrated as in the past, the snow cover on the reflector 8 was removed to measure the reflection characteristics when the measuring device was calibrated. After obtaining the reflection coefficient from the reflection characteristics and obtaining the calibration value, it is necessary to make a flat snow surface again at the time of measurement. However, this work is not necessary. Therefore, it is possible to eliminate the fluctuation of the density inside the snow cover due to human work, and to obtain more accurate measurement data based on natural snow cover.

しかしながら、上記実施例1では、測定用及び校正用アンテナ1、5や測定系及び校正系同軸ケーブル13、14等の測定データに影響を与える測定機器が屋外に設置されているため、長期間の測定の場合には、周囲の環境温度変化による測定系及び校正系同軸ケーブル13、14等の伸縮や風圧振動等による測定用及び校正用アンテナ1、5と反射板7、8との間隔の相対的な位置が変動したり、両アンテナのふらつきかたが異なる等の理由により、校正系と測定系との電気的特性が相違する。   However, in the first embodiment, since measurement devices that affect measurement data such as the measurement and calibration antennas 1 and 5 and the measurement system and calibration system coaxial cables 13 and 14 are installed outdoors, a long-term operation is required. In the case of measurement, the relative distance between the measurement and calibration antennas 1 and 5 and the reflectors 7 and 8 due to expansion / contraction of the measurement system and calibration system coaxial cables 13 and 14 due to a change in ambient environmental temperature, wind pressure vibration, etc. The electrical characteristics of the calibration system and the measurement system differ due to the fact that the general position fluctuates and the way the two antennas fluctuate.

又、校正系の反射板8の周囲には雪の壁面が形成され、校正用アンテナ5に指向性の良いアンテナを使用しても、わずかなアンテナのふらつきのために、反射板8周囲の雪の壁面からの反射波が受信されてしまう。このように、雪の壁面からの反射波を完全に除去出来ず、測定誤差の原因ともなっていた。さらに、第1の実施例では、校正系の反射板8には加熱装置が設置されているので、その消費電力がかかりコストがかさむという問題もある。加熱装置が設置されていない場合には、測定系の反射板7上の除雪は必要ないが、測定使用とする都度、校正系の反射板8上の積雪を除去する必要があり、従来例ほどではないが、手間がかかる等の問題もある。   In addition, a snow wall is formed around the calibration reflector 8, and even if a highly directional antenna is used as the calibration antenna 5, the snow around the reflector 8 may be slightly fluctuated. The reflected wave from the wall surface is received. As described above, the reflected wave from the snow wall cannot be completely removed, which causes a measurement error. Furthermore, in the first embodiment, since a heating device is installed in the calibration reflector 8, there is a problem that the power consumption is increased and the cost is increased. When the heating device is not installed, it is not necessary to remove snow on the reflection plate 7 of the measurement system, but it is necessary to remove snow on the reflection plate 8 of the calibration system each time measurement is used. However, there are also problems such as taking time and effort.

そこで、この発明の第2の実施例では、図4に示すように、校正用アンテナ5と反射板8との代わりに、校正系にスルーの同軸ケーブル(以下、校正用伝送ケーブル20と記す)を用いたもので、以下、図4〜図7に基づいて詳細に説明する。なお、上記実施例1と同一のものは同一符号及び同一名称を用いるとともに、その説明を省略する。   Therefore, in the second embodiment of the present invention, as shown in FIG. 4, instead of the calibration antenna 5 and the reflecting plate 8, a through coaxial cable (hereinafter referred to as a calibration transmission cable 20) is used in the calibration system. Hereinafter, it will be described in detail with reference to FIGS. In addition, the same thing as the said Example 1 uses the same code | symbol and the same name, and abbreviate | omits the description.

図4は第2の実施例を示す構成図、図5は図4の説明図、図6はベクトル図、図7は反射法の幾何学的モデルを示す。測定用アンテナ1は、実施例1と同様に、測定用送信アンテナ1aと測定用受信アンテナ1bとにより構成されており、同軸切換器12と測定用アンテナ1とを接続する測定系同軸ケーブル13と測定用アンテナ1等とにより測定系が構成されている。   FIG. 4 is a block diagram showing the second embodiment, FIG. 5 is an explanatory diagram of FIG. 4, FIG. 6 is a vector diagram, and FIG. 7 shows a geometric model of the reflection method. As in the first embodiment, the measurement antenna 1 includes a measurement transmission antenna 1a and a measurement reception antenna 1b, and a measurement-system coaxial cable 13 that connects the coaxial switch 12 and the measurement antenna 1. A measurement system is constituted by the measurement antenna 1 and the like.

校正系を構成する校正用伝送ケーブル20は、実施例1における校正用アンテナ5と反射板8及び校正用アンテナ5と同軸切換器12とを接続する校正系同軸ケーブル14の代わりに、測定系の電気的特性と全く等しい電気的特性を有する直線状のスルーの同軸ケーブルで形成されている。なお、反射効率を改善するために設置されている反射板としては、実施例1における測定用の反射板7のみが使用される。その他は上記実施例1と同様である。   The calibration transmission cable 20 constituting the calibration system is the same as that of the measurement system in place of the calibration system coaxial cable 14 that connects the calibration antenna 5 and the reflector 8 and the calibration antenna 5 and the coaxial switch 12 in the first embodiment. It is formed of a straight through coaxial cable having electrical characteristics exactly equal to the electrical characteristics. In addition, only the reflecting plate 7 for measurement in Example 1 is used as a reflecting plate installed in order to improve reflection efficiency. Others are the same as in the first embodiment.

この第2の実施例では、図5に示すように、同軸切換器12はネットワークアナライザ15と2本の同軸伝送線路21、22で接続されており、校正用伝送ケーブル20と測定系とを切り換える手段を有しており、測定用アンテナ1の近傍に設置されている。   In the second embodiment, as shown in FIG. 5, the coaxial switch 12 is connected to the network analyzer 15 by two coaxial transmission lines 21 and 22, and switches between the calibration transmission cable 20 and the measurement system. Means and is installed in the vicinity of the measurement antenna 1.

又、図5に示すように、校正用伝送ケーブル20と、測定用送信アンテナ1aと同軸切換器12とを接続する同軸ケーブル23aと、測定用受信アンテナ1bと同軸切換器12とを接続する同軸ケーブル23bとは、同種の線材のケーブルを用いるとともに、同軸ケーブル23aと同軸ケーブル23bとの電気長の和が、校正用伝送ケーブル20の電気長に等しく、線路長も短いほうが望ましい。   Further, as shown in FIG. 5, the calibration transmission cable 20, the coaxial cable 23a for connecting the measurement transmission antenna 1a and the coaxial switch 12, and the coaxial for connecting the measurement reception antenna 1b and the coaxial switch 12 are connected. The cable 23b is preferably a cable of the same type, and the sum of the electrical lengths of the coaxial cable 23a and the coaxial cable 23b is equal to the electrical length of the calibration transmission cable 20 and the line length is preferably short.

図4、図5に基づいて、実際に被測定物3として自然に降り積もった積雪3の誘電率εを求める場合について説明する。
先ず、この第2の実施例の概略を述べると以下の通りである。
即ち、温度変化によるネットワークアナライザ15の変動や同軸ケーブル部分の伸縮等による測定誤差を排除するために、まず、積雪3の無い状態の時に測定用アンテナ1で測定したネットワークアナライザ校正係数から、校正用伝送ケーブル20側に切り換えて得られるネットワークアナライザ校正係数を差し引いたアンテナ間透過係数を求める。更に同様の手順で、測定用送信アンテナ1aと測定用受信アンテナ1bの相対位置を変えず天空方向を向けた状態でのアンテナ間結合係数を測定して、上記アンテナ間透過係数からベクトル的に減算する。これは、基本的にはアンテナ間の結合と同軸ケーブル部分の影響を除いた測定機器校正値を測定したことになり、この値を測定機器校正値の初期値としてパソコン16に保存しておく。そして、この測定機器校正値(初期値)は、測定用アンテナ1のアンテナ特性が変動しないがぎり、固有の値である。
Based on FIGS. 4 and 5, the case where the dielectric constant ε of the snow cover 3 that has actually fallen naturally as the device under test 3 will be described.
First, the outline of the second embodiment will be described as follows.
That is, in order to eliminate measurement errors due to fluctuations in the network analyzer 15 due to temperature changes, expansion / contraction of the coaxial cable portion, etc., first, the network analyzer calibration coefficient measured with the measurement antenna 1 when there is no snow 3 is used for calibration. The inter-antenna transmission coefficient is obtained by subtracting the network analyzer calibration coefficient obtained by switching to the transmission cable 20 side. Further, in the same procedure, the inter-antenna coupling coefficient is measured in the state in which the sky direction is directed without changing the relative position of the measuring transmitting antenna 1a and the measuring receiving antenna 1b, and is subtracted in vector from the inter-antenna transmission coefficient. To do. This basically means that the measurement device calibration value excluding the influence of the coupling between the antennas and the coaxial cable portion is measured, and this value is stored in the personal computer 16 as the initial value of the measurement device calibration value. The measurement device calibration value (initial value) is a unique value as long as the antenna characteristics of the measurement antenna 1 do not fluctuate.

次に、積雪状態において、同軸ケーブル部分の校正値を測定し、保存されている測定機器校正値(初期値)に加算して新たな測定機器校正値(積雪時における校正値)とする方法で、測定用送信アンテナ1aから測定用受信アンテナ1bへの直接波成分による測定誤差、測定時における温度変化によるネットワークアナライザ15の変動や同軸ケーブル部分の伸縮等による校正値誤差をなくし、反射板7と測定用アンテナ1からなる空間開放型の校正系における不安定要素を解消することが出来る。以下、さらに詳細に説明する。   Next, in the snowy condition, measure the calibration value of the coaxial cable part and add it to the stored measuring device calibration value (initial value) to obtain a new measuring device calibration value (calibration value during snowfall). The measurement error due to the direct wave component from the measurement transmission antenna 1a to the measurement reception antenna 1b, the calibration value error due to the fluctuation of the network analyzer 15 due to the temperature change at the time of measurement, the expansion and contraction of the coaxial cable portion, and the like are eliminated. Unstable elements in the open space calibration system comprising the measurement antenna 1 can be eliminated. This will be described in more detail below.

まず、積雪のない状態におけるネットワークアナライザ15の校正法(上記初期値を求める方法)について説明する。この測定では、積雪のない季節に実行され、長期測定時のために取得しておくデータが得られる。
まず、上記初期値を保存する手順は、以下のような手順で実行されて求められる。
(1)換器12を測定用アンテナ1側に切り換えて、レスポンススルー校正を行う。測定用受信アンテナ1bで受信した反射波からネットワークアナライザ15で校正特性を測定し、この校正特性から求めた校正係数C#1(複素数)のデータをパソコン16に保存する。
(2)同軸切換器12を校正用伝送ケーブル20側に切り換えて、レスポンススルー校正を行う。同様にしてネットワークアナライザ15で校正特性を測定し、この校正特性から求めた校正係数C#2(複素数)のデータをパソコン16に保存する。
(3)、校正係数C♯1=|S♯1|εj♯1、校正係数C♯2=|S♯2|εj♯2とすると、測定用送信アンテナ1a及び測定用受信アンテナ1bのコネクタ端からみた透過係数は、
21 =(C#1/C#2)=|S♯1|εj♯1/|S♯2|εj♯2
=|S♯1/S♯2|ε(j♯1−εj♯2)=|S 21|εjφR 21
で表される。従って、透過係数S 21は、校正係数C♯1及び校正係数C♯2から算出出来るがアンテナ間結合を含むのでこれを補正する。
(4)アンテナ間の相対位置を固定したまま、反射板7が存在しない状態、例えば、真上の天空方向に2つのアンテナ開口を向けた状態で、(1)〜(3)の手順を実行して、アンテナ間の結合係数S 21を測定し、保存しておく。この結果、図6に示すように、S 21からS 21をベクトル的に引くことで結合を含まない送受信アンテナ間の透過係数S 21が、S 21=S 21−S 21として求められる。この値は、固有の値であり、測定用アンテナ1の特性(結合度、利得、コネクタ反射特性)が変わらないかぎり、気温変動によりケーブル長が変化した状態で実行して送受信アンテナ間の透過係数S 21値を求めても変動することはない。従って、これを測定時における測定機器校正値の初期値としてパソコン16に保存しておく。
First, a calibration method of the network analyzer 15 (a method for obtaining the initial value) in a state where there is no snow is described. This measurement is executed in a season without snow cover, and data to be acquired for long-term measurement is obtained.
First, the procedure for storing the initial value is obtained by the following procedure.
(1) Switch the converter 12 to the measurement antenna 1 side and perform response-through calibration. The calibration characteristic is measured by the network analyzer 15 from the reflected wave received by the measurement receiving antenna 1b, and the data of the calibration coefficient C # 1 (complex number) obtained from the calibration characteristic is stored in the personal computer 16.
(2) The coaxial switch 12 is switched to the calibration transmission cable 20 side to perform response through calibration. Similarly, the calibration characteristic is measured by the network analyzer 15, and the data of the calibration coefficient C # 2 (complex number) obtained from the calibration characteristic is stored in the personal computer 16.
(3) When the calibration coefficient C # 1 = | S # 1 | εj # 1 and the calibration coefficient C # 2 = | S # 2 | εj # 2 , the transmission antenna for measurement 1a and the reception antenna for measurement 1b The transmission coefficient seen from the connector end is
S 21 R = (C # 1 / C # 2) = | S ♯1 | ε j♯1 / | S ♯2 | ε j♯2
= | S # 1 / S # 2 | ε (j # 1- εj # 2 ) = | S R 21 | ε jφR 21
It is represented by Therefore, the transmission coefficient S R 21 can be calculated from the calibration coefficient C # 1 and the calibration coefficient C # 2, but is corrected because it includes coupling between antennas.
(4) The procedure of (1) to (3) is executed in a state where the reflector 7 is not present with the relative position between the antennas fixed, for example, in a state where the two antenna openings are directed in the sky direction above. Then, the coupling coefficient S D 21 between the antennas is measured and stored. As a result, as shown in FIG. 6, the transmission coefficient S C 21 between the transmitting and receiving antennas that do not contain binding by subtracting from S R 21 and S D 21 vectorially is, S C 21 = S R 21 -S D 21 As required. This value is a unique value. Unless the characteristics of the measurement antenna 1 (coupling degree, gain, connector reflection characteristics) change, the transmission coefficient between the transmitting and receiving antennas is executed with the cable length changed due to temperature fluctuations. Even if the S C 21 value is obtained, there is no change. Therefore, this is stored in the personal computer 16 as the initial value of the calibration value of the measuring device at the time of measurement.

次いで、積雪時における測定は、以下の手順で実行される。
(5)換器12を校正用伝送ケーブル20側に切り換え、レスポンスルー校正を行う。この時ネットワークアナライザ15で校正特性を測定し、この校正特性から求めた校正係数C#2 データを取得する。
(6)校正係数C#2 =|S♯2 |ε φ2 とし、保存してある透過係数S21 との積を求める。
#2 21 =|S♯2 |ε φ2 ・|S21 |εjφC 21=S21
この積S21 が、積雪時における新たなレスポンス校正係数として、ネットワークアナライザ15へ転送される。
(7)次いで、現在の測定データを追跡する。この値が、積雪時に測定した時の実際の測定値となる。
Next, the measurement at the time of snow accumulation is executed according to the following procedure.
(5) The converter 12 is switched to the calibration transmission cable 20 side, and response loop calibration is performed. At this time, the calibration characteristic is measured by the network analyzer 15, and the calibration coefficient C # 2 M data obtained from the calibration characteristic is acquired.
(6) the calibration factor C # 2 M = | S ♯2 M | and ε j φ2 M, obtaining the product of the transmission coefficients S 21 C that are stored.
C # 2 M S 21 C = | S ♯2 M | ε j φ2 M · | S 21 C | ε jφC 21 = S 21 M
This product S 21 M is transferred to the network analyzer 15 as a new response calibration coefficient during snow cover.
(7) Next, the current measurement data is tracked. This value is the actual measured value when measured during snowfall.

このようにして、積雪時における実際の透過係数を求め、この値から反射法により積雪3の透過誘電率εを求める。
この積雪3の透過誘電率εを求めるためには、TE波が積雪面に入射した時の積雪面反射係数ΓTEを精度良く測定する必要がある。以下、積雪面反射係数ΓTEの測定について説明する。
In this way, the actual transmission coefficient at the time of snow accumulation is obtained, and the transmission dielectric constant ε of the snow accumulation 3 is obtained from this value by the reflection method.
In order to obtain the transmission dielectric constant ε of the snow cover 3, it is necessary to accurately measure the snow cover surface reflection coefficient Γ TE when the TE wave is incident on the snow cover surface. Hereinafter, measurement of the snow cover reflection coefficient Γ TE will be described.

ここで、図7に示すように、測定用アンテナ1の送信アンテナ1a及び受信アンテナ1bの両アンテナ高さH、アンテナ指向性利得G、両アンテナ間の間隔をSとする。図7は、校正用の完全反射面を無限大とし、反射板7面上に厚さdの積雪3(誘電率εr=εs-jεs)がある状態を示している。   Here, as shown in FIG. 7, the antenna height H, the antenna directivity gain G, and the distance between the antennas of the transmitting antenna 1a and the receiving antenna 1b of the measuring antenna 1 are S. FIG. 7 shows a state where the calibration complete reflection surface is infinite and there is snow 3 (dielectric constant εr = εs−jεs) having a thickness d on the surface of the reflection plate 7.

測定用送信アンテナ1aから送信電界Etで照射された電波2は、積雪3面で反射し、測定用受信アンテナ1bで受信される。ここで、両アンテナ1a、1bのアンテナ軸Pa、Pは、完全反射面上の反射点Pに向いているものとする。又、送信球面波に対する積雪面反射係数は、平面波入射時の反射係数ΓTEで近似出来る(積雪層内では平面波伝搬と見なす)ものと仮定し、両アンテナ1a、1b間結合(直接波)やアンテナ−積雪面間の多重反射の影響は無視出来るものとする。 The radio wave 2 irradiated with the transmission electric field Et from the measurement transmission antenna 1a is reflected by the surface of the snow 3 and received by the measurement reception antenna 1b. Here, the antenna axis Pa, P b of the antennas 1a, 1b are assumed facing the reflection point P on the fully reflective surface. Also, it is assumed that the snow surface reflection coefficient for the transmitted spherical wave can be approximated by the reflection coefficient Γ TE when the plane wave is incident (considered as plane wave propagation in the snow layer), and the coupling between the antennas 1a and 1b (direct wave) and The influence of multiple reflections between the antenna and the snow cover is negligible.

積雪の無いときの受信電界強度Ermは、下記の式(1)のように示される。 The received electric field strength Erm when there is no snow is shown as the following formula (1).

Figure 0003988828
Figure 0003988828

は自由空間中の伝搬定数、測定に用いた電波のλは波長である。測定用送信及び受信アンテナ利得は、いずれもGとする。積雪3の深さdにおける受信電界Ersは、ΓTEを用いて下記の式(2)で表す。 k 0 is a propagation constant in free space, and λ of the radio wave used for measurement is a wavelength. The measurement transmission and reception antenna gains are both G. The received electric field E rs at the depth d of the snow cover 3 is expressed by the following equation (2) using Γ TE .

Figure 0003988828
Figure 0003988828

従って、無積雪時の受信電界強度Ermを基準とした積雪3の深さdにおける受信電界Ers、即ち測定された伝達特性(反射係数を求めるためのもの)S21は、 Therefore, the received electric field E rs at the depth d of the snow cover 3 with reference to the received electric field strength E rm when there is no snow, that is, the measured transfer characteristic (for obtaining the reflection coefficient) S 21 is:

Figure 0003988828
となる。
Figure 0003988828
It becomes.

ここで、式(3)において、r/rは金属面反射時と積雪面反射時の伝搬線路長差であり、送信球面波の拡散にともなう伝搬損失の比を表し、アンテナ高Hが積雪の深さdに較べて充分長い距離であれば1と見なせる。G(θ)/G(θ)は、金属反射面での入射角度の違いによるアンテナ利得変動比である。これらの2つの項は、1と見なせない場合には、ΓTEの振幅誤差となる。e−j2k(2kD(rs−r)は、伝搬経路長さに伴う位相差分である。測定されたS21は、これらの係数を補正しているので、誘電率を求めるための精度の良い反射係数が得られる。 Here, in the formula (3), r / r s is the propagation path length difference at the time of snow surface reflective metal surface reflection, represents the ratio of the propagation loss due to diffusion of transmission spherical wave, the antenna height H is snow It can be regarded as 1 if the distance is sufficiently longer than the depth d. G (θ S ) / G (θ) is an antenna gain fluctuation ratio due to a difference in incident angle on the metal reflecting surface. These two terms, if not regarded as 1, the amplitude error of the gamma TE. e −j2k (2 kD (rs−r) is a phase difference associated with the propagation path length. Since the measured S 21 corrects these coefficients, it is a highly accurate reflection for obtaining the dielectric constant. A coefficient is obtained.

上記のようにして算出された積雪3の誘電率は、Cバンドの周波数帯で測定された結果であるので、この算出した積雪の誘電率から、VHF〜マイクロ波帯における特定周波数で測定された実験的に導出されている実験式に基づいて、外挿法により空港に設置されているグライドパスの周波数帯に換算して誘電率を算出する。この換算法については、すでに、実施例1において説明したので、その説明を省略する。 Since the dielectric constant of the snow cover 3 calculated as described above is a result of measurement in the C band frequency band, it was measured at a specific frequency in the VHF to microwave band from the calculated dielectric constant of the snow cover . Based on the experimental formula derived experimentally, the dielectric constant is calculated by converting to the frequency band of the glide path installed at the airport by extrapolation. Since this conversion method has already been described in the first embodiment, the description thereof is omitted.

この発明の第1の実施例を示す誘電率測定装置の構成図である。It is a block diagram of the dielectric constant measuring apparatus which shows 1st Example of this invention. この発明の第1の実施例を示すもので、比誘電率の実数部の周波数特性図である。1 is a frequency characteristic diagram of a real part of a relative permittivity according to a first embodiment of the present invention. FIG. この発明の第1の実施例を示すもので、比誘電率の虚数部の周波数特性図である。1 shows a first embodiment of the present invention and is a frequency characteristic diagram of an imaginary part of relative permittivity. FIG. この発明の第2の実施例を示す誘電率測定装置の構成図である。It is a block diagram of the dielectric constant measuring apparatus which shows 2nd Example of this invention. この発明の第2の実施例を示すもので、図4の説明図である。FIG. 5 shows a second embodiment of the present invention and is an explanatory diagram of FIG. 4. この発明の第2の実施例を示すもので、ベクトル図である。FIG. 7 is a vector diagram showing a second embodiment of the present invention. この発明の第2の実施例を示すもので、反射法の幾何学モデル図である。The 2nd Example of this invention is shown and it is a geometric model figure of a reflection method. 従来例を示すもので、透過法による誘電率測定装置の構成図である。It shows a conventional example and is a configuration diagram of a dielectric constant measuring apparatus using a transmission method.

符号の説明Explanation of symbols

1 測定用アンテナ
2 電波
3 被測定物(積雪)
校正用アンテナ
7 反射板
12 同軸切換器
15 ネットワークアナライザ
16 パソコン
20 校正用伝送ケーブル
1 antenna for measurement 2 radio wave 3 object to be measured (snow cover)
5 Calibration antenna 7 Reflector 12 Coaxial switch 15 Network analyzer 16 Personal computer
20 calibration transmission cable

Claims (3)

被測定物に電波を照射し、その反射波から前記被測定物の誘電率を算出する反射法による誘電率の測定方法において、
電気的特性及び形状の等しい測定用送信アンテナと測定用受信アンテナとからなる測定用アンテナとこの測定用アンテナを同軸切換器に接続する同軸ケーブルとを有する測定系と、この測定系の電気的特性と等しい電気的特性を有し、前記同軸切換器に接続されたスルーの校正用伝送ケーブルとをそれぞれ備え、
前記被測定物は、積雪であり、
前記積雪を除去した初期校正時において、
(1)前記同軸切換器を前記測定用アンテナ側に切り換えて測定系における初期の校正特性をネットワークアナライザにより測定し、この初期の校正特性から測定系の初期の校正係数を求め、これを保存し、
(2)次いで、前記同軸切換器を前記校正用伝送ケーブル側に切り換えて、前記ネットワークアナライザにより校正特性を求め、この校正特性から校正系の初期の校正係数を求め、これを保存し、
(3)前記測定系の初期の校正係数から校正系の初期の校正係数を減算して、これを送受信アンテナ間透過係数値として保存し、
(4)前記測定用送信アンテナと前記測定用受信アンテナとの相対位置及び方向を一定にするとともに、前記反射板を除いた状態で、前記各(1)〜(3)の手順に従ってそれぞれアンテナ間結合係数を測定し、前記送信及び受信アンテナ間透過係数値からベクトル的に減算して、測定時校正値の初期値としてこれを保存し、
前記反射板上に前記積雪を載置した状態の測定時において、
)前記同軸切換器を前記校正用伝送ケーブル側に切り換えて前記ネットワークアナライザにより校正特性を測定して、この校正特性から測定時における測定機器校正用の校正係数を求め、
)次いで、この測定機器校正用の校正係数と保存されている前記初期値との積を求め、これを測定時における測定機器校正用の真の反射係数としてネットワークアナライザに転送するとともに、測定データを追跡して、その反射係数を求め、
)この求めた反射係数から前記積雪の誘電率を算出し、
(8)この算出した積雪の誘電率から、VHF〜マイクロ波帯において導出されている実験式に基づいて、外挿法により測定に使用した電波の周波数帯から他の周波数帯における誘電率を算出すること
を特徴とする誘電率の測定方法。
In the measurement method of the dielectric constant by the reflection method of irradiating the measurement object with radio waves and calculating the dielectric constant of the measurement object from the reflected wave,
A measurement system having a measurement antenna comprising a measurement transmission antenna and a measurement reception antenna having the same electrical characteristics and shape, and a coaxial cable connecting the measurement antenna to a coaxial switch, and electrical characteristics of the measurement system Each having a through-calibration transmission cable connected to the coaxial switch,
The object to be measured is snow,
At the time of initial calibration after removing the snow cover ,
(1) Switch the coaxial switch to the antenna side for measurement, measure the initial calibration characteristics in the measurement system with a network analyzer, determine the initial calibration coefficient of the measurement system from the initial calibration characteristics, and save this ,
(2) Next, the coaxial switch is switched to the calibration transmission cable side, the calibration characteristic is obtained by the network analyzer, the initial calibration coefficient of the calibration system is obtained from the calibration characteristic, and stored.
(3) Subtract the initial calibration coefficient of the calibration system from the initial calibration coefficient of the measurement system, and store this as a transmission coefficient value between the transmitting and receiving antennas;
(4) While keeping the relative position and direction of the measurement transmitting antenna and the measurement receiving antenna constant and excluding the reflector, the antennas are respectively connected according to the procedures of (1) to (3). Measure the coupling coefficient, subtract vector-wise from the transmission and reception antenna transmission coefficient value, save this as the initial value of the calibration value at the time of measurement,
At the time of measurement of the state where the snow is placed on the reflector,
( 5 ) Switch the coaxial switch to the calibration transmission cable side, measure the calibration characteristics with the network analyzer, and obtain a calibration coefficient for measuring equipment calibration at the time of measurement from the calibration characteristics,
( 6 ) Next, the product of the calibration coefficient for calibration of the measuring instrument and the stored initial value is obtained, and this is transferred to the network analyzer as a true reflection coefficient for calibration of the measuring instrument at the time of measurement. Trace the data, find its reflection coefficient,
( 7 ) The dielectric constant of the snow is calculated from the obtained reflection coefficient ,
(8) From the calculated dielectric constant of snow, based on the empirical formula derived in the VHF to microwave band, the dielectric constant in other frequency bands is calculated from the frequency band of the radio wave used for measurement by extrapolation. A method for measuring a dielectric constant.
被測定物に電波を照射し、その反射波から前記被測定物の誘電率を算出する反射法による誘電率測定装置において、
前記被測定物は電波を反射する反射板上に降り積もった積雪であり、
電気的特性及び形状の等しい測定用送信アンテナと測定用受信アンテナとからなる測定用アンテナと、
この測定用アンテナを同軸切換器に接続する同軸ケーブルと前記測定用アンテナとを有する測定系が構成され、
この測定系の電気的特性と等しい電気的特性を有し、前記同軸切換器に接続されたスルーの校正用伝送ケーブルと、
ネットワークアナライザに接続され、前記校正用伝送ケーブルと前記測定系とを切り換える手段を有する前記同軸切換器と、
この同軸切換器を介して前記校正用伝送ケーブルと前記測定系とに接続されているとともに、前記校正用伝送ケーブル及び測定系からの校正特性と前記測定系からの反射特性及びアンテナ間結合特性を測定する前記ネットワークアナライザと、
前記反射特性、前記校正特性からそれぞれ校正係数、反射係数を算出する機能と、前記測定機器校正値の初期値を求める機能と、これらの値を保存する機能と、測定した前記積雪の反射係数からこの積雪の誘電率を算出する機能と、算出した積雪の誘電率から、VHF〜マイクロ波帯において導出されている実験式に基づいて、外挿法により測定に使用した電波の周波数帯から他の周波数帯に換算する機能とを備えたパソコンと、
を有することを特徴とする誘電率測定装置。
In a dielectric constant measuring device by a reflection method that irradiates a measured object with radio waves and calculates a dielectric constant of the measured object from the reflected wave,
The object to be measured is snow that has accumulated on a reflector that reflects radio waves,
A measurement antenna comprising a measurement transmission antenna and a measurement reception antenna having the same electrical characteristics and shape;
A measurement system comprising a coaxial cable connecting the measurement antenna to a coaxial switch and the measurement antenna is configured,
An electrical characteristic equal to the electrical characteristic of this measurement system, and a through transmission cable for calibration connected to the coaxial switch,
A coaxial switch connected to a network analyzer and having means for switching between the calibration transmission cable and the measurement system;
The calibration transmission cable and the measurement system are connected to the calibration transmission cable and the measurement system via the coaxial switch, the calibration characteristics from the calibration transmission cable and the measurement system, the reflection characteristics from the measurement system, and the coupling characteristics between the antennas. The network analyzer to be measured;
From the reflection characteristic, a function for calculating a calibration coefficient and a reflection coefficient from the calibration characteristic, a function for obtaining an initial value of the measurement instrument calibration value, a function for storing these values, and a reflection coefficient of the measured snow cover Based on the function to calculate the dielectric constant of this snow cover and the calculated dielectric constant of the snow cover, based on the empirical formula derived in the VHF to microwave band, the frequency band of the radio wave used for the measurement by the extrapolation method and other A personal computer with a function to convert to a frequency band ,
A dielectric constant measuring apparatus comprising:
前記電波の周波数は、Cバンドを用いたこと
を特徴とする請求項に記載の誘電率測定装置。
The dielectric constant measuring apparatus according to claim 2 , wherein a C band is used as a frequency band of the radio wave.
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